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@ARTICLE{Voigt:17012,
author = {Voigt, C. and Schumann, U. and Jessberger, P. and Jurkat,
T. and Petzold, A. and Gayet, J.-F. and Krämer, M. and
Thornberry, T. and Fahey, D.W.},
title = {{E}xtinction and optical depths of contrails},
journal = {Geophysical research letters},
volume = {38},
number = {11},
issn = {0094-8276},
address = {Washington, DC},
publisher = {American Geophysical Union},
reportid = {PreJuSER-17012},
pages = {L11806},
year = {2011},
note = {The CONCERT campaign was organized by the HGF-junior
research group AEROTROP (http://www.pa.op.dlr.de/AEROTROP).
Part of this work was funded within the DLR-project CATS and
by the DFG SPP HALO 1294. We thank the DLR flight
department, the Deutsche Lufthansa (A. Waibel) and DFS for
excellent support. D. Schauble, T. Hamburger, A. Minikin and
J. Gasteiger are thanked for instrument preparation. H.
Schlager provided NOy data. We further thank M. Ponater, C.
Fromming and R. Rodriguez de Leon for stimulating
discussions.},
abstract = {One factor limiting the understanding of the climate impact
from contrails and aircraft induced cloud modifications is
the accurate determination of their optical depth. To this
end, 14 contrails were sampled for 2756 s with instruments
onboard the research aircraft Falcon during the CONCERT
(CONtrail and Cirrus ExpeRimenT) campaign in November 2008.
The young (< 10 min old) contrails were produced by 9
commercial aircraft with weights of 47 to 508 t, among them
the largest operating passenger aircraft, the Airbus A380.
The contrails were observed at temperatures between 214 and
224 K and altitudes between 8.8 and 11.1 km. The measured
mean in-contrail relative humidity with respect to ice was
89 +/- $12\%.$ Six contrails were observed in cloud free
air, the others were embedded in thin cirrus clouds. The
observed contrails exhibited a mean ice water content of 2
mg m(-3) and had a mean number concentration of 117 cm(-3)
and effective radius of 2.9 mu m assuming asphericle
particles with an aspect ratio of 0.5. Probability density
functions of the extinction, with a mean (median) of 1.2
(0.7) km(-1), and of the optical depth tau, with a mean
(median) of 0.27 (0.13), are derived from the in situ
measurements and are likely representative for young
contrails from the present-day commercial aircraft fleet at
observation conditions. Radiative transfer estimates using
the in-situ measured contrail optical depth lead to a
year-2005 estimate of line-shaped contrail radiative forcing
of 15.9 mWm(-2) with an uncertainty range of 11.1-47.7
mWm(-2). Citation: Voigt, C., U. Schumann, P. Jessberger, T.
Jurkat, A. Petzold, J.-F. Gayet, M. Kramer, T. Thornberry,
and D. W. Fahey (2011), Extinction and optical depth of
contrails, Geophys. Res. Lett., 38, L11806,
doi:10.1029/2011GL047189.},
keywords = {J (WoSType)},
cin = {IEK-7},
ddc = {550},
cid = {I:(DE-Juel1)IEK-7-20101013},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK491},
shelfmark = {Geosciences, Multidisciplinary},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000291812900001},
doi = {10.1029/2011GL047189},
url = {https://juser.fz-juelich.de/record/17012},
}